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A NNALES DE L ’I. H. P., SECTION A

G ÉRARD A. M AUGIN

Exact relativistic theory of wave propagation in prestressed nonlinear elastic solids

Annales de l’I. H. P., section A, tome 28, n

o

2 (1978), p. 155-185

<http://www.numdam.org/item?id=AIHPA_1978__28_2_155_0>

© Gauthier-Villars, 1978, tous droits réservés.

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(2)

155

Exact relativistic theory

of

wave

propagation

in prestressed nonlinear elastic solids

Gérard A. MAUGIN

Universite de Paris VI,

Laboratoire de Mecanique Theorique associe au C. N. R. S.,

Tour 66, 4, Place Jussieu, 75230 Paris, Cedex 05, France

Vol. XXVIII, 2, 1978, Physique théorique.

ABSTRACT. - The

propagation

of weak discontinuities in

general

relativistic

prestressed

elastic solids is studied under the sole

hypothesis

that the material be

isotropic

in

an ideally

unstrained state. No limitations

are

placed

upon the

amplitude

of stresses and deformation processes and the formulation has

thermodynamical

foundations. In this

general

frame-

work where the state

equation

for the

potential

has a

quite arbitrary form,

it is shown that

(i) principal

wave fronts are either

longitudinal

or transverse

(the propagation

of

longitudinal

ones

being impeded by

the

possible incompressibility

of the

material); (ii)

in

general,

there may be two transverse waves with distinct

speeds; (iii)

the values of these

speeds

is

expressible

in terms of three

(scalar)

response functions

(typical

of the

material)

and

of the initial

stretches; (iv)

it is

possible

to

give

a relative classification of these values and

(v)

in the case of

propagation through

an initial state of

high hydrostatic

pressure

(case

of dense stellar

objects),

there exists a

universal

relationship

betw een the

simple speed

of

longitudinal

distur-

bances and the double

speed

of transverse ones and the

speed

of sound of a

relativistic

perfect

fluid that would have a law of

compression corresponding

to the initial state. For a sensible

special

case of state

equation

and for an

initial state of

hydrostatic

pressure, the

speeds

of

propagation

and the

speed

of sound referred to above are determined

exactly

in function of two

fundamental scalars of the material and a

density

ratio.

Taking

account

in

supplement

of

perturbations

in the geometry of

space-time,

the same

formalism is

applied

to the construction of

perturbation equations

l’Institut Henri Poincaré - Section A - Vol. XXVIII, 2 - 1978.

(3)

(generalized

Hooke-Navier-Duhamel

equations)

valid either for isothermal

or

isentropic

processes. The latter

equations

are those to be used either in the

study

of « elastic »

gravitational

wave detectors or in the

study

of

small elastic oscillations of dense stellar

objects.

RESUME. 2014 La

propagation

des discontinuites faibles dans les solides

elastiques precontraints

est etudiee dans Ie cadre de la relativité

generate

sous la seule

hypothèse

que Ie materiau soit

isotrope

dans un etat ideal

non deforme. Aucune restriction n’est

imposee

a

1’amplitude

des deforma-

tions et des contraintes et la formulation est basee sur la

thermodynamique.

Dans ce cadre

general

ou

1’equation

d’etat a une

expression

suffisamment

arbitraire,

il est montre que :

(i)

les ondes

principales

sont soit

longitudi-

nales soit transversales

(Fincomprcssibilite possible

du milieu

empechant

la

propagation

des

premières); (ii)

il y a en

general

deux ondes transversales de vitesses

distinctes ; (iii)

la valeur de ces vitesses peut etre

exprimee

en

fonction de trois fonctions de

reponse

scalaires

(typiques

du

materiau)

et

des

elongations initiales ; (iv)

il est

possible

de donner une classification relative de ces vitesses et,

(iv)

dans Ie cas ou la

propagation

a lieu dans un

etat de forte

pression hydrostatique (cas

des

objets

stellaires

denses),

il

existe une relation universelle entre la vitesse

simple

des

perturbations longitudinales,

la vitesse double des

perturbations

transversales et la vitesse du son d’un fluide

parfait

relativiste

qui

aurait une loi de

compression correspondant

a l’état initial. Pour une

expression plausible

de

1’equation

d’etat et un etat initial de

pression hydrostatique,

il est alors

possible

de

determiner exactement les vitesses de

propagation

ainsi que cette vitesse

sonique

en fonction de deux scalaires

caracteristiques

du materiau et d’un rapport de densites. De

plus,

prenant en compte les

perturbations

de

la

geometrie

de

l’espace-temps,

Ie meme formalisme est

employe

a la

construction des

equations

de

perturbation (equations generalisees

de

Hooke-Navier-Duhamel)

valables pour des processus isothermes ou

isentropiques.

Les

equations

ainsi obtenues sont celles

qui

doivent etre

utilisees soit dans l’étude des vibrations

elastiques

des detecteurs d’ondes

gravitationnelles,

soit dans l’étude des

petites

oscillations

elastiques

des

objets

stellaires denses.

1. INTRODUCTION

In papers

[1 ]-[2] recently published

we have studied the

propagation

of infinitesimal discontinuities in certain

simple

classes of relativistic elastic

(or hypoelastic)

bodies. A

study

of the

growth

of the

amplitude

of

such wave fronts

along

their ray has demonstrated the need for an exact

theory requiring

no

hypotheses

as far as the

amplitude

of strains is concerned and

relying

upon a sound

thermodynamics.

It is the purpose of this paper

de Henri Poincaré - Section A

(4)

to present such an exact

theory

with the sole

hypothesis that,

in the case

of

arbitrary

finite

strains,

the

body

be

isotropic

in an

ideally

unstrained

state. The wave

fronts, however,

propagate

through

an

initially

strained

state. For

analytical

convenience the

study

must be limited to that concern-

ing

a

propagation along

a

principal

direction of the initial state of stress.

Since the state

equations

of the elastic bodies to which the present treatment

applies

are, for the

least, badly

known

(e.

g., in neutron

stars),

we concen-

trate upon the derivation of those results which may be said to be universal in the sense that

they

do not

depend explicitly

on the exact form of such a

state

equation.

Having

recalled some basic notions of the

theory

of deformation processes for

general

relativistic matter in

space-time

in Section

2,

we establish in Section 3 the exact form of constitutive

equations

for relati- vistic

isotropic

nonlinear thermoelastic solids.

Following

the definition

of infinitesimal discontinuities in Section

4,

we prove in Section 5 a series of

lemmas,

theorems and corollaries

concerning

universal

(in

the sense

specified above)

results

pertaining

to the

longitudinal

or transverse character of the wave

fronts,

the values of the

speed

of these waves, and the relative classification of these values. In

general

two transverse waves with distinct

speeds

and one

longitudinal

wave can propagate. In

particular,

a universal

relationship

between the

propagation speeds

of

longitudinal

and transverse

wave fronts in an initial state of

high hydrostatic

pressure

(as

may occur in certain

astrophysical objects)

is proven in this

general

framework. The

case of relativistic

incompressible

nonlinear elastic solids which

requires special

attention is

briefly

commented upon in Section 6 where the non-

propagation

of

longitudinal

wave fronts is proven for such bodies. The results are

specialized

in Section 7 for a

special

form of the free energy

density.

There the

speeds

of

propagation

of

longitudinal

and transverse

wave fronts and the

speed

of sound in the case of an initial state of

hydro-

static pressure are determined

exactly

in terms of two fundamental scalars

(analogous

to Lame’s

moduli),

which are characteristic of the

material,

and of the

density

ratio.

By

way of

conclusion,

we deduce in Section

8,

from the exact

expressions

established

before,

the

generalization

of Hooke’s

law to be used in the treatment of small elastic oscillations either in

« elastic »

gravitational-wave

detectors or in

astrophysical objects

acted

upon

by

their own

gravitational

field. The

Appendices provide

lists of

coefficients as also a brief

comparison

between constitutive

equations proposed by

different authors for the

description

of relativistic elastic

matter

( 1 ).

Basic results

reported

in this paper have been enunciated in a

short Note

[4].

Related

previous

works

using

a different

formalism,

which

e) The brief review given in a preceding paper ([3], Appendix) written in 1971-1972

now is obsolete.

Vol. XXVIII, n° 2 - 1978.

(5)

either are based on too

specialized hypotheses

or fall short of the conclusions reached in the present paper, are those of Bressan

[5],

Grot

[6] (in special relativity),

and Carter

[7].

2.

PREREQUISITES

2.1. Notation

Let M =

(V4,

be a

space-time

of

general relativity equipped

with

a normal

hyperbolic metric

ga~

(x, ~ == 1, 2, 3, 4 ;

index 4

time-like ;

Lorentzian

signature + , + , + , - ).

ux is the

four-velocity

such that

1

(c

= 1 for notational

convenience). ~~

and

oa

denote the

partial

and covariant derivatives with respect to the local chart x03B1 of M.

D =

u03B1~03B1

is the invariant derivative in the direction of M".

P03B103B2

= g03B103B2 + u03B1u03B2 is the

spatial projector

which is used

systematically

in the

following

deve-

lopment

to write down the local canonical

space-time decomposition

of

any tensor field defined on M. The local

spatial projection

of any

geometrical object

A is noted

A1

and admits u as zero vector for all its indices in a local chart.

Objects

such that A =

A1

are said to be

spatial.

The transverse or

spatial

covariant derivative is defined

by oa

=

22 Deformation of matter in

space-time

Following Maugin [8]

and Carter and

Quintana [9],

we admit that the motion of a relativistic continuum is described either

by

means of a canonical

differentiable

projection P

such that P :

G[B] ~

N or with the aid of the

space-time parametrized

congruence of world lines ~ : x =

~(X, T),

X E

B,

1" e !R. Here

F[B]

is the open tube of y4 which is swept out

by

the

material

body

B

(whose

constituents are the material «

particles » X)

and

(V3, K,

L =

1, 2, 3,

is the three-dimensional manifold which serves to describe the material continuum. B is an open

region

of T is the proper time of X. ~ is

equipped

with the local

background

metric

GKL

and local charts

XK,

K =

1, 2,

3. We have thus

These relations are assumed to possess a sufficient

degree

of

continuity

and

differentiability

in their arguments so as to allow for the

forthcoming manipulations.

For

instance,

one can define the inverse motion

gradient X~

by

°‘~ being

the

reciprocal

of a

space-time

invariant noted

C L

but

tensor field on ~~~ 2014 is constructed

by applying

the

projection ~ :

Annales de l’Institut Henri Poincaré - Section A

(6)

This defines the relativistic

analogue

of the Piola finite-strain tensor of classical continuum mechanics

(Compare [lO], Chap. I).

Its

geometrical significance

is clear. It is the

image

of the

space-time

metric

by

the

projection

of the

space-time

on its

quotient by

the congruence

(2.1)3’

Furthermore, assuming

that the Jacobian determinant of

(2 .1 )3 keeps

the same

sign (e.

g.,

plus)

in the course of the relativistic motion of X and

defining

the direct motion

gradient xK by

the chain rule of differentiation

yields

and it is

possible

to define the strain tensor

CKL

such that =

ði

and

Let

Gxa

be the

image

of

GKL

in M

by f!JJ, i.

e.,

Then we can define two useful tensor fields which serve to measure finite strains either on N or on M,

EKL

and such that

[3] [77] ]

and

Elementary computations [3], [72]

then allow one to establish the

following

results that relate

propertime

rates of

change

of different

geometrical objects

of interest :

and where

and

Vol. XXVIII, 2 - 1978. 11

(7)

for any

spatial

tensor

Aaa

= denotes the Lie derivative with respect to the field u. In terms of the differentiable

projection 9,

we have

Equation (2 .12)2

is a consequence of

Eqs. (2.12)i, (2 . 7)

and

(2.10).

This

shows that

G«~

is the

background

metric on

M,

which serves as a local standard to measure strains.

According

to

Eqs. (2.12)

and

(2.14),

the

Herglotz-Born

local condition of

rigid-body

motion is defined in diffe- rential form

(Killing’s theorem) by

either one of the

following

conditions :

2.3. Field

equations

In

supplement

to Einstein’s field

equations

that relate

linearly

the

Einstein tensor and the total energy-momentum tensor, we have

Here

p(x)

=

p(X, T)

is the mass per unit of proper volume. In absence of heat

conduction, electromagnetic

fields and

spin

the energy-momentum

tensor admits the

following simple

canonical space-time decomposi- tion :

where t03B103B2 = t03B203B1, as a consequence of

Eq. (2.20)2,

is the

spatial

relativistic

stress tensor, and E is the internal energy per unit of proper mass.

Taking

account of

Eq. (2.19)

and of the fact that =

0,

we

project Eq. (2.20)i along

u~ and

orthogonally

to u to obtain

and where

is the tensorial index of the

continuum,

cf. Ref.

[2].

In the present case the local statement of the second

principle

of

thermodynamics

reduces to the

equation Dry

=

0, where ~

is the entropy per unit of proper mass.

Introducing

the

specific

free energy

t/J by

= s 2014 where 8 is the proper thermo-

dynamical

temperature

(o

&#x3E;

0,

inf 8 =

0),

we can rewrite

Eq. (2.22)

in

the form

Annales de l’Institut Henri Poincaré - Section A

(8)

3. CONSTITUTIVE

EQUATIONS

FOR ISOTROPIC THERMOELASTIC BODIES

A natural definition for

general

thermoelastic bodies

(i.

e., with a

priori large deformations)

is

given by postulating

a functional

dependence

of the

form

.

That

is,

there are no

hereditary

effects since

dependent

and

independent

variables are considered at the same event

point

of M or,

equivalently,

for the same values of the four parameters

(XK, -r).

Then we have the

THEOREM 3 .1. - The exact constitutive

equations o, f ’

an

anisotropic

thermoelastic

body

are

given by

03C8 satisfying

0 the

following

0 set

of first

order linear

partial differential

tions:

It then follows the

L __

COROLLARY 3.2.

Equations (3.2)

and

(3.3)

can be

replaced by

i. e., the image by P

of TKL ~ (~03C8/~ Ch) = TLK

up to the

2014

Consider ~

=

0)

to start

with,

then compute with the

help

of

Eq. (2.10)i

to obtain

if c~ =

Furthermore, according

to the

principles

of formulation

set forth

by

the

Author, 03C8

must be

objeetive,

i. e., its

explicit

form should

not

depend

on the observer

[12], [l3].

We have shown that in the present

case which does not involve

hereditary effects,

this invariance is

equivalent

to the rotational Lorentz invariance of

L~

in a local inertial

frame,

or

else,

to invariance under all generators of

SO(3)

in local nonholonomic

spatial

frames

along

~.

Studying

such a form invariance for

8)

under

infinitesimal

transformations xa ===

+ in

special relativity

or

under infinitesimal rotations = =

1, 2, 3,

between

rigid

Vol. XXVIII, 2 - 1978.

(9)

spatial

triads at an event

point

of

M,

where * indicates

validity

in

inertial frames

only,

e is an

infinitesimally

small and

L~a

is

arbitrary,

and

recasting

the

resulting equation

in a

complete

covariant

framework,

we are led to the condition

(3 . 3).

On account of

this, Eq. (3.5) simplifies

and the

expression

of

03C1D03C8 being

carried in

Eq. (2.25)

which is

posited

to be valid for any DB and all deformation fields that do not

rigidify

the continuum in the sense of

Herglotz

and Born

(i.

e.,

0), completes

the

proof

of Theorem 3.1. The system of differential

equations (3.3) integrates immediately along

its characteristics if

~ depends

on

X~ only through

the

space-time

invariant combination Hence the

proof

of

Corollary 3.2; Q.

E. D.

Equations (3.4)

are the

equations

deduced pre-

viously

from a variational

principle by

the Author

[8].

Equations (3.4)

and those

equivalent equations

which are discussed

in

Appendix

I describe

anisotropic

thermoelastic bodies. The notion of material symmetry which relies upon

cristallography

is

essentially

a three-

dimensional Euclidean

notion,

i. e., it concerns the

study

of the invariance

of functions with respect to members of

subgroups

of the group

0(3).

Since,

as a result of

Corollary 3.2, ~r depends

now

only

on arguments defined on 8

being

a parameter, material symmetry must be discussed in the local tangent space to ~l at X.

However,

we shall avoid this

compli-

cation in the

sequel

for we shall use

only

arguments defined on M to faci- litate the

analysis

of wave-front

propagation.

In

fact, using

the result

enunciated in Theorem

3.1,

we can state the

THEOREM 3.3. -

a)

The exact constitutive

equations of’

an

isotropic

relativistic thermoelastic

body

are

given by

either

or

depending

on

whether ~

or E is used as

thermodynamical potential.

b)

and B are

isotropic functions [in

the sense of

SO(3)]

of

the

relativistic finite-strain

tensor ~.

Proof

2014 We

can write Eq. (2.9)

in the form

Note that

depends

on

X~

via

X~

itself and via

CMN

that

depends

on

~

hence on its

reciprocal X~ .

It follows

by varying Eq. (2.5)i

1 that

Anna/es de Henri Poincaré - Section A

(10)

From

Eq. (2.6)

it follows that

Then

Eq. (3.8) yields

on account of

Eqs. (2.5). Then,

if one makes the

change

of

independent

variables

~(X~0) ~ Eq. (3.11)

substituted in

Eqs. (3.2)i

and

(3 . 3) yields Eq. (3.6)1 and,

on account of the symmetry of the

following

system of first order linear

partial

differential

equations

similar

equations involving 8

instead

of 03C8

are obtained

by performing

the

partial Legendre

transformation e

= ~

+ As is

readily checked, Eq. (3.12)

is but the covariant

expression

of the fact

that ~

must be

objective,

i. e., form-invariant

by SO(3)

in a local inertial frame. In such a frame

Eq. (3.12)

is satisfied

identically if 03C8 depends

on E

only through

its funda-

mental invariants

Ik

= tr

~k,

tr =

trace, k

=

1, 2,

3. Since these are space- time

invariants,

the result holds

good

in

fully

covariant formalism. This

means

that 03C8

or E is an

isotropic

function of its tensorial argument, 8 or ~

acting

as a

simple

parameter. The

body

thus described exhibits no

preferred spatial

direction as far as its response to deformations is concerned. It is

isotropic ; Q.

E. D.

Applying

the

Cayley-Hamilton

theorem it then is

possible

to restate the

foregoing

result as

COROLLARY 3.4. - The exact constitutive

equations of

an

isotropic

relativistic thermoelastic

body

are

given in

intrinsic notation

by

where the

gr’s

are

space-time

invariant scalars

and, by

convention,

(~°)°‘a =

On account of the

expression given

in

Appendix

II for the scalars gr,

Eq. (3.13)1

is the relativistic version of the constitutive

equation

derived

by Murnaghan [l4]

in classical

isotropic elasticity

with finite deformations.

Remark that this

equation

is universal in the sense that 8 is a

general

func-

tion of the invariants

Ik,

whose

expression

can be constrained

only by

some

regularity assumptions,

some conditions of elastic

stability

and the condi-

tions of relativistic

causality

and the

required reality

of wave

speeds,

the

latter

being

determined in

following

sections.

Vol. XXVIII, 2 - 1978.

(11)

Remark.

2014 (f)

The manner in which the

equations

above have been obtained guarantees that

they

are valid in

special relativity,

and at the

nonrelativistic

limit,

in classical continuum

mechanics,

and

that,

in

supple-

ment to the

objectivity requirement

of the

Author, they satisfy identically

the

rheological

invariance

proposed by Oldroyd [15]

for

general

relativistic continuous matter.

Remark.

- (ii)

A direct

proof

of

Eqs. (3.13)

can be

given by starting

with the a

priori

functional

dependence ~(~ap, 8). Then,

in

computing

one uses

Eq. (2.16)

to pass from to hence to

daa

in virtue

of

Eq. (2.14). Taking

account of the

decomposition

of ea~ in

symmetric

and

skewsymmetric

parts, one is thus led to

Applying

the same argument as that

applied

in the

proof

of Theorem

3 .1,

but for the

objectivity of 03C8

as a function of it results

Eq. (3.12).

Hence

Eq. (3.14) simplifies,

and it remains to substitute for the

expression

of

provided by

this

simplified equation,

into

Eq. (2.25)

to arrive at the

results

(3.6).

4. DEFINITION

OF INFINITESIMAL DISCONTINUITIES

We recall the definitions introduced in a

previous

work

[16] (See

also

Lichnerowicz

[77]).

Let = 0 be the time-like

hypersurface

that represents a

discontinuity

front which propagates in V4 and thus separates

~ _

F[B]

in two

subregions

and at each time. We set

and

~ is the

(nondimensional) speed

of the

discontinuity

front measured relati-

vely

to the

moving matter. l"

is oriented from the « minus » to the «

plus »

side of W. A + and A -

being

the uniform limits of A in

approaching

W on

its two

faces, we note [A] =

A+ - A-. If

A,

g03B103B2 and u03B1 are continuous

across Wand

if 03B4

denotes the Dirac distribution with compact support

on

W,

then we can write -

and

where the field ðA is called the infinitesimal

discontinuity

of A

through

W.

We call the

two-plane

orthogonal

to the unit

spatial

vector

,

Annales de l’Institut Henri Poincare - Section A

(12)

S«~ = P«~ - !~«~’~,a

is the covariant

projector

on to

H~~.

The canonical

decomposition

of any

spatial geometrical object along

the direction of ~, and on to

H~

is obtained

by applying

the operator

S,

e. g., with an obvious notation and obvious

properties

for the elements of

decomposition

thus

introduced,

Similar

decompositions hold good

for

f«~

and with the elements of

decomposition F«, F)

and

E«, E), respectively.

We call

Ø’[B]

c

M) == {p,

~, 17, u«, a solution of the

system of

equations

formed

by

Einstein’s field

equations, Eqs. (2.19)

and

(2.23),

the constitutive

equations (3 .13)

and the condition

D17

= 0

(provided

that such a solution

exists;

this difficult

problem

of existence is not

approached

in this

paper).

Then the wave fronts that we consider in the

forthcoming

sections

satisfy

the

following

set of

hypotheses :

Hi :

any

typical

solution is continuous across

W;

H2 :

except for the metric all

space-time

derivatives of the first order of the fields of the solution suffer discontinuities across W

(the

case where 0

requires

a

special study);

H3 :

W is not a

gravitational

wave

front,

i. e., ~2 - 1 is

excluded;

.

H4 :

W is not a material wave front or, in other

words,

since

D17 = 0 yields ~~~

= 0 in agreement with

Eq. (4.5)~,

W is not an entropy

front,

i. e., ~ = 0 is excluded so that

~r~

= 0

necessarily.

In virtue of

H..1,

W is not a shock wave since

~u«~ ~

0. In virtue of

H3

and

H4

the admissible range for GlC is limited to the open interval

]0,1[ c= ~

if ~ is to be real and less than the

light velocity

in vacuum

(relativistic causality).

We call

principal

wave fronts those wave fronts for

which ~,«

coincides

with an

eigenvector

of the initial state of stress E

According

to

Eq. (3.13)i,

if W is such a wave

front,

then the

corresponding ~,«

coincides

also with an

eigenvector

of the initial state of strain E

Naturally,

this holds true

only

for

isotropic

bodies.

Longitudinal

wave fronts are those

wave fronts for which

(~u ~ 0, ~u1

=

0),

and transverse wave fronts are

those for which

(5M

=

0, 0).

We shall not consider

general

wave

fronts which may be called mixed wave fronts

(Cf. [2] ).

5. PRINCIPAL WAVE FRONTS

IN ISOTROPIC RELATIVISTIC THERMOELASTIC BODIES We consider

only principal

wave fronts except in

degenerate

cases of

initial state of stress where the character or

principalness

has no

meaning.

In

general

admits three distinct

orthogonal (with

respect to the metric

eigenvectors (spatial

unit

four-vectors) ~=1,2,3,

Vol. XXVIII, 2 - 1978.

(13)

with

corresponding eigenvalues ~.

For a

principal

wave front

W,

let

d~ 1,

coincides with A.

d~ 1 ~

is also an

eigenvector

of Let

t{ 1 ~

be the

corresponding

stress

eigenvalue and E~

the

corresponding

strain

eigenvalue. Then t~

and

E~

are related

by

the

equation

The

remaining

two

eigenvectors

of both

ta~

and and

d~3~,

form an

orthonormal

dyad

on which can be

projected

any tensorial

object

A such

that

S(A)

= A. Then we can set the

following

lemma.

LEMMA 5.1. -

Principal (infinitesimal discontinuity)

wave

fronts

W

that

propagate in

an

isotropic

relativistic thermoelastic

body

are either

purely longitudinal

or

purely

transversal.

Proof.

A

straightforward

calculation

yields

the

following expression (written

in intrinsic

formalism)

for the

right-hand

side of

Eq. (2.23)

on

account of

Eq. (3.13)1 :

where

gr(Ik, ~) -

and the nine scalars which are functions

of

Ik and ~ only,

are listed in

Appendix

III.

Now consider the infinitesimal discontinuities of

Eqs. (2.19), (2.23)

and of

(~~

on account of the definition

(2.16)

and of

Eq. (5.2). Taking

account of the fact that

fa~

and are continuous across Wand

using

the

definitions

(4.1) through (4.5)

and

Eq. (5.1),

we

obtain,

with ~ ~

0,

and

Annales de l’Institut Henri Poincaré - Section A

(14)

where

n writmg /) we nave taken accoum 01 me results (5.5), (5. 5) anu

(5.6)

and of the fact that

51]

= 0.

Upon using

the

decompositions (4.6)

and

(4. 7)

and the

analogous decompositions

for

fa~

and

~a~

and

accounting

for the fact

that, being

an

eigenvector

of and it also is an

eigen-

vector of the

projection

of

Eq. (5.7) along

the direction of A

yields

~’ F - {(1 - 2~)~ - ~

+

2~~1)

+

2~(1 - 2~)} ~~u = 0, (5 . 9)

with 2

whereas its

projection

onto reads

the mixed

projection vanishing identically

for

fa

=

Fa

=

Ea

=

0 ;

hence

the

proof

of Lemma 5 .1. That

is,

we have

uncoupling

between

longitudinal

and transverse wave fronts because

(i)

of the

isotropy

of the

body

and

(ii)

of the

principalness

of the wave front.

Since

p ~ 0,

we can state at once the

following

theorem :

THEOREM 5.2. -

Longitudinal principal

wave

fronts

that

propagate in

an

isotropic

relativistic thermoelastic

body

have a

speed

such that

where

is the

principal

stretch in the

spatial

direction whereas transverse

principal

wave

fronts

in

generat

have two distinct

speeds, uT2

and

uT3,

which are

so utions

0

the

equation

where

Equation (5.14)

is solved

immediately

in the nonholonomic frame

(d(2~,

where

diagonalizes. Setting .f’2

=

F.2, 3

=

F?3, ~2

=

E.2, ~3 = E33,

and i;, =

( 1 - 2~)’~~ ~’

=

2, 3,

the solutions of

(5.14)

are

given by

Vol. XXVIII, n° 2 - 1978.

(15)

For the wave

speeds

to be real and less than

unity,

the

right-hand

side

of

Eqs. (5.12)

and

(5.16)

must be in the interval

]0,

1

[.

This

clearly imposes

constraints on the initial state

9Mo

i. e., on rather

complex

combinations of the response functions gr and the initial strains and

stretches,

and vk.

Apart

from those

constraints,

the results enunciated in the form of

Eqs. (5.12)

and

(5.16)

are universal since

they

do not

depend

on any assump- tion as

regards

the

amplitude

of strains

(e.

g.,

they

are valid

for finite strains)

and on any

particular

functional

dependence

of the internal energy E

(Ik, ri),

which of course possesses a sufficient

regularity.

A

general study

of the

constraints referred to above cannot be

performed

under the

hypothesis

of

a

general

initial state. Neither can it be achieved a relative classification of the two transverse wave

speeds

in an exact manner in such a

general

frame-

work. The

approximate following results, however,

can be established.

Let us define

Ak, k

=

2, 3, by

Then with the definition

of vk

we can

give

the

following

form to the diffe-

rence

~T2 - ~3:

Of course,

f2 ~ /3 ==

1 +

0(c-2)

&#x3E;

0,

so that we can introduce a mean

value f

for

f2 and f3

and rewrite

(5.18)

as

The

Ak

are all

positive

from their very

definition,

and vi &#x3E; v~

yields Ai A~.

We have thus

COROLLARY 5.3.

- a)

Transverse wave

fronts

with

amplitude paraltet

to the axis

of

lesser transverse stretch travel at a greater absotute

speed

than others

if,

with gl 1 &#x3E;

0,

i)

either g2 0 and 1 -

f(A2

+

A3) g1/g21, ii)

Or g2 &#x3E; 0 and

f(A2

+

A3) -

1

b)

Transverse wave

fronts

with

amptitude parattel

to the axis

of

greater

transverse stretch travet at a greater absotute

speed

than others

if,

with gl &#x3E;

0, i)

either g2 0 and

,f’(A2

+

A3) -

1

g1/g2,

ii)

Or g2 &#x3E; o and 1 -

(A2

+

A3) g1/g2 I

c)

The two types

of

wave

front

travel at the same absolute

speed if

and

only if

the

corresponding

transverse stretches are

equal.

The result

c)

is exact and does not

require

the

approximation (5.19).

Statements

a)

and

b)

follow from the discussion of the

sign

of the

right-

hand side of

Eq. (5.19).

The reason

why

we have considered gl &#x3E; 0 is made clear as follows.

Another

possibility

for

expressing

the difference

~T2

--

~T~

is obtained

Annales de l’Institut Henri Poincare - Section A

(16)

by reintroducing

the

principal

stresses

t(2~

and

t(3~

via an

equation

of

the

type

of

Eq. (5.1)

for those

quantities

in terms of the

eigenvalues ~2

and

~3.

We have

and

Hence, Eq. (5.20)

takes the form

if

where

is Lame’s modulus and CT is a

typical

transverse-wave

speed.

g 2’ == 0 represents one part of the neo-Hookean

assumption (stress-strain

constitutive relation at most

explicitly

linear in

F). Equation (5.23)

is

similar to an

equation given

in our

previous

work

[2].

It says that transverse

wave fronts with

amplitude parallel

to the axis of lesser transverse stress travel at a greater absolute

speed

than the others. The other part of the neo-Hookean

assumption

is obtained

by looking

at

Eq. (5.18) which,

with

the

approximation

made

above,

takes the same form as

Eq. (5.23)

if and

only 03C1g1/2v2,

where v is a

typical

transverse stretch.

Since

is

experi- mentally

shown to be

positive (and

must in fact be so

according

to the

thermodynamics

of neo-Hookean

materials),

and

v2

&#x3E;

0,

then gl must be greater than zero.

By

the same token the definition

(5 .24)2

makes sense.

In conclusion of

this, point

a

representation

of neo-Hookean materials is obtained for

The statement

c)

of

Corollary

5.3 holds

good

in certain

degenerate

cases of initial stresses and

strains,

for

instance, i )

if this state is a

cylindri- cally symmetric

one about the direction and

ii)

if this initial state is

spherical,

that

is, fully degenerate,

in which case the above-obtained results

apply although

the notion of

principalness

has lost its

meaning.

Such an

initial state

is,

for

instance,

an initial state of

high hydrostatic

pressure, as

can arise in the «

geophysics »

of neutron stars

(See

Ruderman

[7~]). Regard- ing

this

special

case the

following

remarkable result can be arrived at.

THEOREM 5 . 4. -

(simple) speed u~ and the (double) speed 0, f longitudinal

and transverse wave

.f’ronts

that

propagate in

an

isotropic

relativistic nonlinear elastic

body, of

which the initial state is one

of high

Vol. XXVIII, n° 2 - 1978.

(17)

hydrostatic

pressure po

(case of

dense stellar

objects),

are related

by

the

universal

relationship

,

^

where

and

a

being

the sound

speed,

and

f

the index

(in

the sense of

Lichnerowicz), of

a retativistic

perfect fluid

that would have the same taw

of compression.

~’roof.

We are in a

fully degenerate

case for which

with

where ~~! = C2

= C. Set v =

( 1 - 2~) -1 ~2

the

isotropic

stretch in the state

9Ko.

Then the matter proper

density

and the same

density

in an

ideally

unstrained state, p~i~, are related

by

the

equation

= 3.

We deduce thus

and

by applying

the chain rule of differentiation. It follows from

(5.30)

and

(5.32)

that

whereas

Eqs. (5.12)

and

(5.16)

reduce to

and

respectively,

on account

of Eq. (5.31)

and o of the definition

(5.28)1.

Substi-

Anna/es de l’Institut Henri Poineare - Section A

(18)

tuting

from

(5. 33)

into

(5.34)

and

combining (5. 34)

and

(5. 35) completes

the

proof. Q.

E. D.

The exact result

(5.26)

valid within the relativistic framework of finite- strain

theory

is universal for no

hypotheses

need be made

concerning

the

explicit

functional form of the internal energy function. It consists in the

general

relativistic

generalization

of a classical result due to Truesdell

[19].

In the neo-Hookean case described

by Eq. (5 . 25)

it reduces to the

equation proposed by

Carter

[7].

It is reasonable to assume that &#x3E; 0.

Therefore,

in

general, ~ ~2 ~~ &#x3E; -

Relativistic

causality

thus

imposes

that

(4/3)~lCl

+ 1. That

is,

It is difficult to establish the

reality

of but the

following

can be

pointed

out :

COROLLARY 5.5.

- If

transverse wave

fronts

can propagate at all in

an

isotropic

retativistic nontinear elastic

body in an

initial

state of hydro-

static pressure, then

longitudinal

wave

.f’ronts

can propagate as welt.

Indeed,

if

u2|

&#x3E;

0,

then

U2~

&#x3E;

a2

&#x3E; 0.

However,

if

U2|

0

(no

propaga- tion of transverse

fronts),

then

~~~

a2 and

~~~

can be zero or

imaginary,

so that the case

~~j

0

(no propagation

of

longitudinal

wave

fronts)

cannot a

priori

be excluded.

In the neo-Hookean case the

causality

condition

(5.36)

takes on the

simple

form

(with

=E

For a

body

unable to support

shearing effects,

hence for

,u

=

0,

this last

inequality

reduces to that

given

in relativistic

hydrodynamics (Cf.

Israel [20] ).

6. REMARK ON THE INCOMPRESSIBLE CASE

Typical

materials for which the

foregoing development applies

are those

which make up the thick crust of neutron stars, of which the outer

portion probably

resembles terrestrial matter except that it is about

1018

times more

rigid

than steel and much more

incompressible,

so that it is easier to

jiggle

it than to compress it

(Cf. [8], [21 ] ).

Conclusions

regarding

this

limiting

case can be drawn

directly

from the results of

previous

sections. If the relativistic elastic

body

is

incompressible,

then the deformations it suffers

are isochoric. This is

expressed

in terms of the strain tensor

by

the

condition

Vol. XXVIII, 2 - 1978.

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